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Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Short-term Evaporation Estimating from 
Complex Small Lakes in (Semi-)Arid Regions 
Ali Abbasi 
Nick van de Giesen 
Delft University of Technology 
Water Resources Management 
August 20, 2014 
1 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Outline 
1 Introduction 
Evaporation 
Estimating Evaporation 
2 The Proposed Approach 
Advantages 
Approach Theory 
Application of CFD 
CFD Scenarios 
Framework 
3 Case Study: Lake Binaba 
Description 
4 Simulation Process 
CFDEvapModel-ToolBox 
5 Results 
Results 
6 Conclusion 
Conclusion 
2 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Evaporation 
Evaporation 
Why do we need to estimate Evaporation? 
As a major component of the hydrologic cycle. 
The largest one of water loss from lakes, especially in arid and 
semi-arid regions. 
Approximately one half of the stored water in shallow lakes may 
be lost due to evaporation 
Aects the storage eciency of small lakes, 
Evaporation  Food Security 
Determining the evaporation precisely is critically important to 
assessing the reliability of small reservoir in arid regions. 
3 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Estimating Evaporation 
Estimating Evaporation 
Accurately estimate evaporation from water bodies: 
The key element to make improvements in water storage 
(reservoir) management 
Estimating or measuring evaporation over a lake or reservoir is a 
very dicult task 
The required meteorological parameters rarely measured over the 
water surface. 
The thermal lag between the water body and land surfaces 
renders 
The land-based measurements inecient in parameterization of 
open water evaporation 
Evaporation: from Lake vs. from Land 
Lake evaporation is largely uncoupled from the land 
evapotranspiration 
4 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Estimating Evaporation 
Methods 
A wide range of methods are available to estimate evaporation: 
Measurements: evaporation pan,eddy correlation technique. 
Mass balance(budget)method. 
Energy budget methods. 
Mass transfer method. 
Combination methods. 
Temperature and radiation base methods 
CFD-based approach. 
5 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Estimating Evaporation 
Complexity 
Estimating evaporation from water surface is ...!! : 
Perhaps the most dicult component of all the hydrological cycle 
components 
Complex interactions between the components of the 
lake-atmosphere system 
Being a function of: 
meteorological and climatological factors(temperature, relative 
humidity, wind speed, etc.) 
geology and physiography of water bodies(size, depth, shape, 
advective, location, etc.) 
Evaporation: a unique feature of each lake 
Due to dependency of evaporation on these parameters, it is a unique 
feature of each lake and developing a clearly an unique theoretical 
method for its estimation could be inhibited 
6 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Estimating Evaporation 
Complexity 
With respect to evaporation, lake and reservoirs quite dierent from 
land surfaces: 
The penetrating of suns energy into the water 
Mixing the water column by surface motion 
The large heat storage capacity of water 
The density of water (approximately 1000 times dense more 
dense than air) 
Nearly constant evaporation rate for night and day 
7 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Estimating Evaporation 
Complexity 
Evaporation from water surface 
8 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Outline 
1 Introduction 
Evaporation 
Estimating Evaporation 
2 The Proposed Approach 
Advantages 
Approach Theory 
Application of CFD 
CFD Scenarios 
Framework 
3 Case Study: Lake Binaba 
Description 
4 Simulation Process 
CFDEvapModel-ToolBox 
5 Results 
Results 
6 Conclusion 
Conclusion 
9 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Advantages 
Advantages 
The propose approach is: 
Based on mass-transfer(aerodynamic) method. 
Moderate input data demands 
A generalisable and cost eective approach 
Using Computational Fluid Dynamics(CFD)as a very powerful 
tool. 
Assuming heat and mass transfer analogy 
Drive convective heat transfer coecient and mass-transfer 
coecients for a given water body 
The spatial variation of the evaporation rate over the water 
surface 
Consider the advection eects under arid climate conditions 
CFDEvapModel: CFD-based Evaporation Approach 
Dierent Climate conditions, the Spatial Distribution of Evaporation 
over the Water Surface and the eects of advection(oasis) over the 
water surface 
10 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Approach Theory 
Approach Theory 
Based on the mass-transfer(aerodynamic) method 
E = f(u)(es  ea) 
f(u2) = a + bu2 
Not all of the known processes are included in wind function. 
Constants a and b are vary with climate, lake size, etc. 
full-scale experiments can provide realistic wind function for 
speci
c water bodies. 
11 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Approach Theory 
Approach Theory 
The convective heat exchange between the air and the water surface: 
Hs = hs(Tw  Ta) = 
Nu  k 
L 
(Tw  Ta) 
The evaporation rate from a water surface: 
Elake = 
Sh  D  (Xs  Xa) 
L 
Analogy between the mass and heat transport processes: 
Nu 
Prn = 
Sh 
Scn 
) hm = 
Sh:D 
L 
= 
Nu:Scn:D 
L:P rn = 
hs:Scn:D 
k:P rn 
Mass transfer coecient(hm) is extracted from the heat transfer 
coecient(hs) and consequently evaporation can be estimated from 
water surface. 
12 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Application of CFD 
Application of CFD 
Computational Fluid Dynamics(CFD) is used to: 
Have a precise and applicable estimation of transfer coecients. 
Simulating the air 
ow and heat transfer over the water 
surface(in ABL) 
Dierent and complex con
guration of lake and its surroundings 
can be analysed. 
Very high spatial resolution data are obtained. 
Dierent conditions of ABL can be considered(from stable to 
unstable conditions). 
13 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Application of CFD 
Air Flow over the Water Surface 
Continuity Equations 
@uj 
@xj 
= 0; (1) 
Momentum Equation 
@ui 
+ 
@t 
@ 
@xj 
(ujui)  
@ 
@xj 
 
eff 
 
@ui 
@xj 
+ 
@uj 
@xi 
 
 
2 
3 
 
@uk 
@xk 
 
ij 
 
=  
@p 
@xi 
+ gi [1
(T  Tref )] 
Temperature Equation 
@T 
@t 
+ 
@ 
@xj 
(Tuj)  eff 
@ 
@xk 
( 
@T 
@xk 
) = 0 
14 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Application of CFD 
CFD Computational Domain 
Computational domain with the boundaries 
15 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Application of CFD 
CFD Computational Domain 
Generated computational Mesh for CFD simulation 
16 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Application of CFD 
Boundary Conditions 
boundary conditions of the CFD model of ABL 
Location boundary condition 
Inlet boundary u = u 
 ln 
 
z+z0 
z0 
 
v = 0 w = 0; 
k = u2 
p 
C 
r 
C1  ln 
 
z+z0 
z0 
 
+ C2; 
 = u3 
 
(z+z0) 
r 
C1  ln 
 
z+z0 
z0 
 
+ C2; 
@ 
@z (T) = 0 
Outlet boundary @ 
@x (u; v;w; k; ; T) = 0; 
Lateral boundaries v = 0; @ 
@y (u;w; k; ; T) = 0; 
Top boundary w = 0; @ 
@z (u; v; k; ; T) = 0; 
Terrain boundary (u; v;w) = 0; @ 
@z (T) = 0 Standard(rough)Wallfunctions; 
Lake boundary (u; v;w) = 0; @ 
@z (T) = 0; Standard(smooth)Wallfunctions; 
17 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Application of CFD 
Generating CFD Mesh 
Generating a good computational grid is essential. 
Concentration of grid points near the the lake boundary is more 
clustered to cover the sharp gradients in resolved parameters 
In this work, the mesh was generated with the SnappyHexMesh 
utility available in OpenFOAM. 
making balance between computational time and quality of the 
simulated results. 
18 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
CFD Scenarios 
De
ning Scenarios 
De
ning scenarios regarding most important parameters: 
Water surface temperature(Ts) 
Air temperature(Ta) 
Wind speed over the water surface(U2) 
Atmospheric stability condition() 
19 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
CFD Scenarios 
De
ning Scenarios 
Dierent scenarios for CFD simulations 
CFD Scenario Ta[C] Tw[C] RH[%] U2[m=s] [] stability condition 
CFDEvap-01 37.7 32.073 25 0.50 11.963 stable 
CFDEvap-02 37.7 32.073 25 1.50 0.8042 stable 
CFDEvap-03 37.7 32.073 25 2.50 0.2522 stable 
CFDEvap-04 37.7 32.073 25 5.00 0.0516 stable 
CFDEvap-05 19.9 29.34 85 0.50 -34.916 unstable 
CFDEvap-06 19.9 29.34 85 1.50 -4.156 unstable 
CFDEvap-07 19.9 29.34 85 2.50 -1.482 unstable 
CFDEvap-08 19.9 29.34 85 5.00 -0.317 unstable 
20 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Framework 
Framework 
Lake Borders 
(Points Cloud) 
 Dimensions 
of the 
CFD Domain 
Preparing the CFD Computational Domain 
Volume Mesh 
Generation 
(blockMesh  
snappyHexMesh) 
CFD Simulation 
System 
Regression for 
Different Scenarios 
(wind function) 
Visualization 
The Results 
Producing 
Graphs 
 Figures 
To Analyse 
Simulations 
Results(CFD) 
Pre-processing 
Setting up the 
Boundary 
Conditions 
Numerical Setup 
And 
Physical Parameters 
Using T_a,T_w,RH 
Calculating X_a,X_s 
Heat and Mass Transfer Calculations 
Surface Cleaning 
and Reduction 
(MehsLAb  addMESh) 
Surface 
Reconstruction 
(Generating STL) 
Calculating 
Convective Heat 
Transfer 
Coefficient(h_s) 
Calculating 
Convective 
Mass Transfer 
Coefficient(h_m) 
Calculating 
Distribution of 
Evaporation 
Over the water Surface 
Calculating 
Heat Flux(H_s) over 
water Surface 
Proposed CFD-based simulation to calculate evaporation from the water surface 
21 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Outline 
1 Introduction 
Evaporation 
Estimating Evaporation 
2 The Proposed Approach 
Advantages 
Approach Theory 
Application of CFD 
CFD Scenarios 
Framework 
3 Case Study: Lake Binaba 
Description 
4 Simulation Process 
CFDEvapModel-ToolBox 
5 Results 
Results 
6 Conclusion 
Conclusion 
22 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Description 
Description 
Lake Binaba: 
Location: an arti
cial lake located in northern Ghana 
Surface: the average area of the lake surface is 4.5 km2 
Average depth: only 3 m 
Maximum depth: 7 m 
Usage: a small reservoir, used as a form of infrastructure for the 
provision of water 
Air temperature: 
uctuates between 24 C and 35 C 
Water surface temperature: varies from 28 C to 33 C 
Climate: (semi-)arid region 
23 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Description 
Location 
Lake Binaba: 
Figure: Location of lake Binaba 
r 
24 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Description 
Location 
Lake Binaba: 
Figure: Location of lake Binaba(Google earth) 
25 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Outline 
1 Introduction 
Evaporation 
Estimating Evaporation 
2 The Proposed Approach 
Advantages 
Approach Theory 
Application of CFD 
CFD Scenarios 
Framework 
3 Case Study: Lake Binaba 
Description 
4 Simulation Process 
CFDEvapModel-ToolBox 
5 Results 
Results 
6 Conclusion 
Conclusion 
26 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
CFDEvapModel-ToolBox 
Tools 
using powerful, open-source and free of charge tools: 
27 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
CFDEvapModel-ToolBox 
OpenFOAM 
OpenFOAM: Open Source Field Operation and 
Manipulation 
Open-Source Library 
Free of Charge 
Running in LINUX OS 
C++ Library 
Linking with PYTHON 
New solvers and BCs can be implemented by the user 
Running in parallel on distributed processors 
28 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Outline 
1 Introduction 
Evaporation 
Estimating Evaporation 
2 The Proposed Approach 
Advantages 
Approach Theory 
Application of CFD 
CFD Scenarios 
Framework 
3 Case Study: Lake Binaba 
Description 
4 Simulation Process 
CFDEvapModel-ToolBox 
5 Results 
Results 
6 Conclusion 
Conclusion 
29 / 37
Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion 
Results 
Results 
Distribution of sensible and latent heat 
uxes over the water surface 
30 / 37

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CFD-based Evaporation Estimation Approach

  • 1. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Short-term Evaporation Estimating from Complex Small Lakes in (Semi-)Arid Regions Ali Abbasi Nick van de Giesen Delft University of Technology Water Resources Management August 20, 2014 1 / 37
  • 2. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Outline 1 Introduction Evaporation Estimating Evaporation 2 The Proposed Approach Advantages Approach Theory Application of CFD CFD Scenarios Framework 3 Case Study: Lake Binaba Description 4 Simulation Process CFDEvapModel-ToolBox 5 Results Results 6 Conclusion Conclusion 2 / 37
  • 3. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Evaporation Evaporation Why do we need to estimate Evaporation? As a major component of the hydrologic cycle. The largest one of water loss from lakes, especially in arid and semi-arid regions. Approximately one half of the stored water in shallow lakes may be lost due to evaporation Aects the storage eciency of small lakes, Evaporation Food Security Determining the evaporation precisely is critically important to assessing the reliability of small reservoir in arid regions. 3 / 37
  • 4. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Estimating Evaporation Estimating Evaporation Accurately estimate evaporation from water bodies: The key element to make improvements in water storage (reservoir) management Estimating or measuring evaporation over a lake or reservoir is a very dicult task The required meteorological parameters rarely measured over the water surface. The thermal lag between the water body and land surfaces renders The land-based measurements inecient in parameterization of open water evaporation Evaporation: from Lake vs. from Land Lake evaporation is largely uncoupled from the land evapotranspiration 4 / 37
  • 5. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Estimating Evaporation Methods A wide range of methods are available to estimate evaporation: Measurements: evaporation pan,eddy correlation technique. Mass balance(budget)method. Energy budget methods. Mass transfer method. Combination methods. Temperature and radiation base methods CFD-based approach. 5 / 37
  • 6. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Estimating Evaporation Complexity Estimating evaporation from water surface is ...!! : Perhaps the most dicult component of all the hydrological cycle components Complex interactions between the components of the lake-atmosphere system Being a function of: meteorological and climatological factors(temperature, relative humidity, wind speed, etc.) geology and physiography of water bodies(size, depth, shape, advective, location, etc.) Evaporation: a unique feature of each lake Due to dependency of evaporation on these parameters, it is a unique feature of each lake and developing a clearly an unique theoretical method for its estimation could be inhibited 6 / 37
  • 7. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Estimating Evaporation Complexity With respect to evaporation, lake and reservoirs quite dierent from land surfaces: The penetrating of suns energy into the water Mixing the water column by surface motion The large heat storage capacity of water The density of water (approximately 1000 times dense more dense than air) Nearly constant evaporation rate for night and day 7 / 37
  • 8. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Estimating Evaporation Complexity Evaporation from water surface 8 / 37
  • 9. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Outline 1 Introduction Evaporation Estimating Evaporation 2 The Proposed Approach Advantages Approach Theory Application of CFD CFD Scenarios Framework 3 Case Study: Lake Binaba Description 4 Simulation Process CFDEvapModel-ToolBox 5 Results Results 6 Conclusion Conclusion 9 / 37
  • 10. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Advantages Advantages The propose approach is: Based on mass-transfer(aerodynamic) method. Moderate input data demands A generalisable and cost eective approach Using Computational Fluid Dynamics(CFD)as a very powerful tool. Assuming heat and mass transfer analogy Drive convective heat transfer coecient and mass-transfer coecients for a given water body The spatial variation of the evaporation rate over the water surface Consider the advection eects under arid climate conditions CFDEvapModel: CFD-based Evaporation Approach Dierent Climate conditions, the Spatial Distribution of Evaporation over the Water Surface and the eects of advection(oasis) over the water surface 10 / 37
  • 11. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Approach Theory Approach Theory Based on the mass-transfer(aerodynamic) method E = f(u)(es ea) f(u2) = a + bu2 Not all of the known processes are included in wind function. Constants a and b are vary with climate, lake size, etc. full-scale experiments can provide realistic wind function for speci
  • 12. c water bodies. 11 / 37
  • 13. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Approach Theory Approach Theory The convective heat exchange between the air and the water surface: Hs = hs(Tw Ta) = Nu k L (Tw Ta) The evaporation rate from a water surface: Elake = Sh D (Xs Xa) L Analogy between the mass and heat transport processes: Nu Prn = Sh Scn ) hm = Sh:D L = Nu:Scn:D L:P rn = hs:Scn:D k:P rn Mass transfer coecient(hm) is extracted from the heat transfer coecient(hs) and consequently evaporation can be estimated from water surface. 12 / 37
  • 14. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Application of CFD Application of CFD Computational Fluid Dynamics(CFD) is used to: Have a precise and applicable estimation of transfer coecients. Simulating the air ow and heat transfer over the water surface(in ABL) Dierent and complex con
  • 15. guration of lake and its surroundings can be analysed. Very high spatial resolution data are obtained. Dierent conditions of ABL can be considered(from stable to unstable conditions). 13 / 37
  • 16. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Application of CFD Air Flow over the Water Surface Continuity Equations @uj @xj = 0; (1) Momentum Equation @ui + @t @ @xj (ujui) @ @xj eff @ui @xj + @uj @xi 2 3 @uk @xk ij = @p @xi + gi [1
  • 17. (T Tref )] Temperature Equation @T @t + @ @xj (Tuj) eff @ @xk ( @T @xk ) = 0 14 / 37
  • 18. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Application of CFD CFD Computational Domain Computational domain with the boundaries 15 / 37
  • 19. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Application of CFD CFD Computational Domain Generated computational Mesh for CFD simulation 16 / 37
  • 20. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Application of CFD Boundary Conditions boundary conditions of the CFD model of ABL Location boundary condition Inlet boundary u = u ln z+z0 z0 v = 0 w = 0; k = u2 p C r C1 ln z+z0 z0 + C2; = u3 (z+z0) r C1 ln z+z0 z0 + C2; @ @z (T) = 0 Outlet boundary @ @x (u; v;w; k; ; T) = 0; Lateral boundaries v = 0; @ @y (u;w; k; ; T) = 0; Top boundary w = 0; @ @z (u; v; k; ; T) = 0; Terrain boundary (u; v;w) = 0; @ @z (T) = 0 Standard(rough)Wallfunctions; Lake boundary (u; v;w) = 0; @ @z (T) = 0; Standard(smooth)Wallfunctions; 17 / 37
  • 21. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Application of CFD Generating CFD Mesh Generating a good computational grid is essential. Concentration of grid points near the the lake boundary is more clustered to cover the sharp gradients in resolved parameters In this work, the mesh was generated with the SnappyHexMesh utility available in OpenFOAM. making balance between computational time and quality of the simulated results. 18 / 37
  • 22. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion CFD Scenarios De
  • 24. ning scenarios regarding most important parameters: Water surface temperature(Ts) Air temperature(Ta) Wind speed over the water surface(U2) Atmospheric stability condition() 19 / 37
  • 25. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion CFD Scenarios De
  • 26. ning Scenarios Dierent scenarios for CFD simulations CFD Scenario Ta[C] Tw[C] RH[%] U2[m=s] [] stability condition CFDEvap-01 37.7 32.073 25 0.50 11.963 stable CFDEvap-02 37.7 32.073 25 1.50 0.8042 stable CFDEvap-03 37.7 32.073 25 2.50 0.2522 stable CFDEvap-04 37.7 32.073 25 5.00 0.0516 stable CFDEvap-05 19.9 29.34 85 0.50 -34.916 unstable CFDEvap-06 19.9 29.34 85 1.50 -4.156 unstable CFDEvap-07 19.9 29.34 85 2.50 -1.482 unstable CFDEvap-08 19.9 29.34 85 5.00 -0.317 unstable 20 / 37
  • 27. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Framework Framework Lake Borders (Points Cloud) Dimensions of the CFD Domain Preparing the CFD Computational Domain Volume Mesh Generation (blockMesh snappyHexMesh) CFD Simulation System Regression for Different Scenarios (wind function) Visualization The Results Producing Graphs Figures To Analyse Simulations Results(CFD) Pre-processing Setting up the Boundary Conditions Numerical Setup And Physical Parameters Using T_a,T_w,RH Calculating X_a,X_s Heat and Mass Transfer Calculations Surface Cleaning and Reduction (MehsLAb addMESh) Surface Reconstruction (Generating STL) Calculating Convective Heat Transfer Coefficient(h_s) Calculating Convective Mass Transfer Coefficient(h_m) Calculating Distribution of Evaporation Over the water Surface Calculating Heat Flux(H_s) over water Surface Proposed CFD-based simulation to calculate evaporation from the water surface 21 / 37
  • 28. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Outline 1 Introduction Evaporation Estimating Evaporation 2 The Proposed Approach Advantages Approach Theory Application of CFD CFD Scenarios Framework 3 Case Study: Lake Binaba Description 4 Simulation Process CFDEvapModel-ToolBox 5 Results Results 6 Conclusion Conclusion 22 / 37
  • 29. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Description Description Lake Binaba: Location: an arti
  • 30. cial lake located in northern Ghana Surface: the average area of the lake surface is 4.5 km2 Average depth: only 3 m Maximum depth: 7 m Usage: a small reservoir, used as a form of infrastructure for the provision of water Air temperature: uctuates between 24 C and 35 C Water surface temperature: varies from 28 C to 33 C Climate: (semi-)arid region 23 / 37
  • 31. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Description Location Lake Binaba: Figure: Location of lake Binaba r 24 / 37
  • 32. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Description Location Lake Binaba: Figure: Location of lake Binaba(Google earth) 25 / 37
  • 33. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Outline 1 Introduction Evaporation Estimating Evaporation 2 The Proposed Approach Advantages Approach Theory Application of CFD CFD Scenarios Framework 3 Case Study: Lake Binaba Description 4 Simulation Process CFDEvapModel-ToolBox 5 Results Results 6 Conclusion Conclusion 26 / 37
  • 34. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion CFDEvapModel-ToolBox Tools using powerful, open-source and free of charge tools: 27 / 37
  • 35. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion CFDEvapModel-ToolBox OpenFOAM OpenFOAM: Open Source Field Operation and Manipulation Open-Source Library Free of Charge Running in LINUX OS C++ Library Linking with PYTHON New solvers and BCs can be implemented by the user Running in parallel on distributed processors 28 / 37
  • 36. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Outline 1 Introduction Evaporation Estimating Evaporation 2 The Proposed Approach Advantages Approach Theory Application of CFD CFD Scenarios Framework 3 Case Study: Lake Binaba Description 4 Simulation Process CFDEvapModel-ToolBox 5 Results Results 6 Conclusion Conclusion 29 / 37
  • 37. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Results Results Distribution of sensible and latent heat uxes over the water surface 30 / 37
  • 38. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Results Results Relationship between wind speed and transfer coecients: 31 / 37
  • 39. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Results Results Estimated sensible and latent heat uxes using proposed approach: 32 / 37
  • 40. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Results Results Estimated sensible and latent heat uxes using proposed approach: 33 / 37
  • 41. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Outline 1 Introduction Evaporation Estimating Evaporation 2 The Proposed Approach Advantages Approach Theory Application of CFD CFD Scenarios Framework 3 Case Study: Lake Binaba Description 4 Simulation Process CFDEvapModel-ToolBox 5 Results Results 6 Conclusion Conclusion 34 / 37
  • 42. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Conclusion Conclusion CFD is a powerful tool in analysing and designing water resources issues. The proposed methodology represents an useful framework in estimating evaporation for water bodies. the eects of advection and atmospheric instability are considered. the spatial distributions of sensible and latent heat uxes over the water surface can be estimated. using the proposed approach is easily applicable and cost eective in estimating evaporation from the water surface. 35 / 37
  • 43. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Conclusion Thanks Thanks for your attention 36 / 37
  • 44. Introduction The Proposed Approach Case Study: Lake Binaba Simulation Process Results Conclusion Conclusion Questions? More details: a.abbasi@tudelft.nl 11th International Conference on Hydroinformatics(HIC 2014) August 2014 New York City, USA 37 / 37